TY - CONF

T1 - HS EVOLUTION IN HUMIFICATION PROCESS

AU - Chukov, Serafim

PY - 2014

Y1 - 2014

N2 - HS are obligatory participants of not only terrestrial and water ecosystems in small biological circle, but also and in the big geological circle at a level biosphere and geosphere as a single whole. Although quantitatively they compose a little more than half of soil organic matter content in soils and ground waters, their role in functioning of containing them ecosystems immeasurably exceeds their quantitative participation. HS are the unique natural accumulator of the biochemical energy created by green plants during the uptake the of Sun energy due to photosynthesis. In this connection the problem of estimation of evolutionary trends of HS is important not only for soil science, but also for a lot of related subjects: biology, geology, etc. We carried out researches of soils HS structurally functional parameters in soils of natural climatic belts from taiga up to a forest-steppe and steppe. Investigations have been compiled both in natural, and antropogenically altered soils - arable and buried. The data

AB - HS are obligatory participants of not only terrestrial and water ecosystems in small biological circle, but also and in the big geological circle at a level biosphere and geosphere as a single whole. Although quantitatively they compose a little more than half of soil organic matter content in soils and ground waters, their role in functioning of containing them ecosystems immeasurably exceeds their quantitative participation. HS are the unique natural accumulator of the biochemical energy created by green plants during the uptake the of Sun energy due to photosynthesis. In this connection the problem of estimation of evolutionary trends of HS is important not only for soil science, but also for a lot of related subjects: biology, geology, etc. We carried out researches of soils HS structurally functional parameters in soils of natural climatic belts from taiga up to a forest-steppe and steppe. Investigations have been compiled both in natural, and antropogenically altered soils - arable and buried. The data

KW - soil organic matter

KW - humic substances

M3 - Abstract

SP - 115

EP - 116

T2 - Третья международная конференция СНГ МГО HIT-2014/Десятая международная конференция daRostim 2014 «Гуминовые вещества и другие биологически активные соединения в сельском хозяйстве»

Y2 - 18 November 2014 through 22 November 2014

ER -